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Peru · Stratovolkan

Huaynaputina

Tipe
Stratovolkan
Ketinggian
4679 m
Letusan terakhir
1600
Huaynaputina is a relatively inconspicuous volcano that was the source of one of the largest historical eruptions of the central Andes in 1600 CE.  The volcano has no prominent topographic expression.  This view is from the east into a 2.5-km-wide complex caldera that is breached widely to the east.  Three ash cones, one of which can be seen in the shadow at the right-center, are located on the floor of the caldera.  Light-colored ash deposits from the 1600 eruption can be seen mantling the caldera rim.
Huaynaputina is a relatively inconspicuous volcano that was the source of one of the largest historical eruptions of the central Andes in 1600 CE. The volcano has no prominent topographic expression. This view is from the east into a 2.5-km-wide complex caldera that is breached widely to the east. Three ash cones, one of which can be seen in the shadow at the right-center, are located on the floor of the caldera. Light-colored ash deposits from the 1600 eruption can be seen mantling the caldera rim. · Foto: Photo by Oscar González-Ferrán (University of Chile).
Tipe
Stratovolkan
Negara
Peru
Wilayah
Amerika Selatan / Central Andean Volcanic Arc
Ketinggian
4679 m
Koordinat
-16.614, -70.854
Letusan terakhir
1600
Kondisi tektonik
Zona subduksi / Kerak benua (> 25 km)
Bentuk lahan
Komposit
Batuan utama
Dasit
Ringkasan geologi

Huaynaputina (whose name means "new volcano") was the source of the largest historical eruption of South America in 1600 CE. It has no prominent topographic expression and lies within a 2.5-km-wide collapse depression and further excavated by glaciers within a Tertiary to Pleistocene edifice. Three overlapping ash cones with craters up to 100 m deep were constructed during the 1600 CE eruption on the floor of the older crater, whose outer flanks are heavily mantled by ash deposits from the 1600 eruption. This powerful fissure-fed eruption may have produced nearly 30 km3 of dacitic tephra, including pyroclastic flows and surges that traveled 13 km to the E and SE. Lahars reached the Pacific Ocean, 120 km away. The eruption caused substantial damage to the major cities of Arequipa and Moquengua.

Ringkasan Wikipedia

Ringkasan Inggris

Huaynaputina is a volcano in a volcanic high plateau in southern Peru. Lying in the Central Volcanic Zone of the Andes, it was formed by the subduction of the oceanic Nazca Plate under the continental South American Plate. Huaynaputina is a large volcanic crater, which lacks an identifiable mountain profile, with an outer stratovolcano and three younger volcanic vents within an amphitheatre-shaped structure that is either a former caldera or a remnant of glacial erosion. The volcano has erupted dacitic magma.

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Riwayat letusan

2 tercatatGlosarium
Ringkasan (VEI dari waktu ke waktu)
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7750 SM~7438 SM · 1 letusan · VEI maks. ?1288~1600 · 1 letusan · VEI maks. 67750 SM5568 SM3075 SM893 SM1288

Garis waktu rinci

  1. 1600VEI 6Teramati
    1600-02-17 – 1600-03-06
    Summit and south flank
  2. 7750 SM (±200 tahun)VEI ?Perkiraan geologi
    7750 SM – akhir tidak diketahui

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